東西に分割した北太平洋指数の観点から見た総観気候学的特性
The Aleutian Low is a low pressure system which prevails over the Aleutian Islands mainly during the winter season. North Pacific Index (NPI) is known as an index of the strength of the Aleutian low (Trenberth and Hurrel,1994). This study examined the characteristics of the NPI, by which the subject...
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日本大学文理学部自然科学研究所
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ftnihonuniv:oai:repository.nihon-u.ac.jp:11263/2363 2023-06-11T04:03:19+02:00 東西に分割した北太平洋指数の観点から見た総観気候学的特性 Synoptic Climatological Features from a Viewpoint of the North Pacific Index Divided into the East and the West 花戸, 佑輔 山川, 修治 2019-03-05 application/pdf https://repository.nihon-u.ac.jp/xmlui/handle/11263/2363 https://doi.org/10.15006/chs20201054013 jpn ja jpn 日本大学文理学部自然科学研究所 03693562 https://repository.nihon-u.ac.jp/xmlui/handle/11263/2363 doi:10.15006/chs20201054013 Aleutian Low North Pacific Index (NPI) California Niño blocking pattern Pacific-North American (PNA) pattern Departmental Bulletin Paper 2019 ftnihonuniv https://doi.org/10.15006/chs20201054013 2023-06-01T23:44:55Z The Aleutian Low is a low pressure system which prevails over the Aleutian Islands mainly during the winter season. North Pacific Index (NPI) is known as an index of the strength of the Aleutian low (Trenberth and Hurrel,1994). This study examined the characteristics of the NPI, by which the subject area was divided into west sector and east sector, which was defined as ENPI and WNPI, respectively. Around the Hawaiian Islands, the amount of precipitation increased/decreased during the positive/negative WNPI phase. In the tropical eastern Pacific, sea surface temperature (SST) became lower/higher than an average in the positive/negative ENPI phase. Especially, significant positive anomalies were seen on the California coast in the negative ENPI phase. These characteristics are referred to as the California Niño (Yuan and Yamagata, 2014), which is considered to exert a considerable influence on the transportation of water vapor on the West coast of North America. In general, the Pacific-North American (PNA) pattern tends to develop in the positive/negative WNPI and ENPI phase, respectively. It was recognized that in the Northern hemisphere, a blocking pattern tends to be established when WNPI and ENPI are in the positive or negative phase. Report aleutian low Aleutian Islands Nihon University Repository Pacific |
institution |
Open Polar |
collection |
Nihon University Repository |
op_collection_id |
ftnihonuniv |
language |
Japanese |
topic |
Aleutian Low North Pacific Index (NPI) California Niño blocking pattern Pacific-North American (PNA) pattern |
spellingShingle |
Aleutian Low North Pacific Index (NPI) California Niño blocking pattern Pacific-North American (PNA) pattern 花戸, 佑輔 山川, 修治 東西に分割した北太平洋指数の観点から見た総観気候学的特性 |
topic_facet |
Aleutian Low North Pacific Index (NPI) California Niño blocking pattern Pacific-North American (PNA) pattern |
description |
The Aleutian Low is a low pressure system which prevails over the Aleutian Islands mainly during the winter season. North Pacific Index (NPI) is known as an index of the strength of the Aleutian low (Trenberth and Hurrel,1994). This study examined the characteristics of the NPI, by which the subject area was divided into west sector and east sector, which was defined as ENPI and WNPI, respectively. Around the Hawaiian Islands, the amount of precipitation increased/decreased during the positive/negative WNPI phase. In the tropical eastern Pacific, sea surface temperature (SST) became lower/higher than an average in the positive/negative ENPI phase. Especially, significant positive anomalies were seen on the California coast in the negative ENPI phase. These characteristics are referred to as the California Niño (Yuan and Yamagata, 2014), which is considered to exert a considerable influence on the transportation of water vapor on the West coast of North America. In general, the Pacific-North American (PNA) pattern tends to develop in the positive/negative WNPI and ENPI phase, respectively. It was recognized that in the Northern hemisphere, a blocking pattern tends to be established when WNPI and ENPI are in the positive or negative phase. |
format |
Report |
author |
花戸, 佑輔 山川, 修治 |
author_facet |
花戸, 佑輔 山川, 修治 |
author_sort |
花戸, 佑輔 |
title |
東西に分割した北太平洋指数の観点から見た総観気候学的特性 |
title_short |
東西に分割した北太平洋指数の観点から見た総観気候学的特性 |
title_full |
東西に分割した北太平洋指数の観点から見た総観気候学的特性 |
title_fullStr |
東西に分割した北太平洋指数の観点から見た総観気候学的特性 |
title_full_unstemmed |
東西に分割した北太平洋指数の観点から見た総観気候学的特性 |
title_sort |
東西に分割した北太平洋指数の観点から見た総観気候学的特性 |
publisher |
日本大学文理学部自然科学研究所 |
publishDate |
2019 |
url |
https://repository.nihon-u.ac.jp/xmlui/handle/11263/2363 https://doi.org/10.15006/chs20201054013 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
aleutian low Aleutian Islands |
genre_facet |
aleutian low Aleutian Islands |
op_relation |
03693562 https://repository.nihon-u.ac.jp/xmlui/handle/11263/2363 doi:10.15006/chs20201054013 |
op_doi |
https://doi.org/10.15006/chs20201054013 |
_version_ |
1768378633587523584 |